It is probably worth taking a quick look at the waveform
recording system used by Krider, Leteinturier, and Willett to
recording lightning E and dE/dt signals. A block diagram of
their system is shown below. At the time digital waveform
recorders were just becoming available. Prior to that analog
signals were displayed on oscilloscopes and the oscilloscope
display was photographed with a (film) camera. The signals
weren't digitized. The hybrid system below includes both old
(oscilloscopes) and new (digitizers).
You should recognize the flat plate E field
antennas shown at the top of the figure. Separate
antennas were used for dE/dt, Fast E, a 5 MHz RF signal, and a
Slow E signal. The signal cables from the Fast E and
Slow E antennas were connected to integrators. We
discussed all of this earlier in the semester so that should
be familiar.
For dE/dt, the cable from the flat plate antenna (the left
most antenna above) was not connected to an integrator.
Rather it was connected to a 50 ohm resistor, the
characteristic impedance of the coaxial cable. The
voltage that appears across this resistor is proportional to
dE/dt as shown below.
Note the dE/dt signal cable is here shown connected to the
internal trigger of the storage oscilloscope (the 5 MHz RF
signal was also used to trigger the storage
oscilloscope). The dE/dt signal then ran through a 45 m
length of coaxial cable before being connected to the input of
the storage oscilloscope. The 45 m length of cable acted
as a delay line (about 150 ns of delay). The hope was
that with sufficient "pretrigger" signal you could establish
an accurate zero. The figure below shows an
oscilloscope display of a signal with and without delay.
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The oscilloscope begins to sweep when the signal crosses the
trigger threshold. Without delay you would only capture
a portion of the rise to peak (left figure). With
sufficient delay (right figure) you could capture the entire
front edge of the signal.
Some examples of dE/dt signals recorded with a system like the
one above are shown below at left. An E signal obtained
by integrating the dE/dt waveforms is shown at right. LS
and RS indicate leader step and return stroke signals
respectively.
The dE/dt signals were recorded on a very fast time
base. A storage oscilloscope was oscilloscope signal if
a storage scope hadn't been used. The red line shown at
the left of each of the dE/dt signals shows the approximate
storage oscilloscope trigger level.
It is much easier to obtain pretrigger signal when using a
waveform digitizer. A waveform digitizer continuously
digitizes the incoming signal. It doesn't attempt to
store all of this data only the most recent samples. As
new data is acquired and added to the memory, the oldest data
is pushed out of the memory. Once a trigger signal is
received, the digitizer collects a preset number of additional
samples and then stops recording. The data in memory is
preserved until it can be read or displayed (both were done in
the system above).
As best I can remember the waveform digitizers above had the
following characteristics
Model number
|
resolution
|
maximum sampling rate
|
memory size
|
Biomation 805
|
8 bits
|
5 MHz (0.2 μs/sample)
|
2048
|
Biomation 1010
|
10 bits
|
10 MHz (0.2 μs/sample) |
?
|
Biomation 8100
|
8 bits
|
100 MHz (10 ns/sample)
|
?
|
Biomation 1015
|
?
|
100 kHz (10 μs/sample) |
?
|